Helium isotope ratios in Easter microplate basalts

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Basalt, Earth Mantle, Helium Isotopes, Ocean Dynamics, Oceanography, Plumes, Tectonics, Volcanoes, Anomalies, Chemical Composition, Geochemistry, Mid-Ocean Ridges, Pacific Ocean

Scientific paper

He-3/He-4 ratios in Easter Microplate basalt glasses show clear evidence of the effects of a mantle plume. The East Rift of the microplate between 26 and 28 deg S, identified by La/Sm, Sr and Pb isotopes and ridge crest elevation as the region of maximum plume influence, has He-3/He-4 ratios spanning the entire range from 7.5 to 11.7 R(sub A). The Easter Microplate is the only section of the entire East Pacific Rise that is associated with a known `hotspot' track (mantle plume) and has elevated He-3/He-4 ratios. Although most of the West Rift basalts contain MORB helium (8.0 - 8.7 (R sub A)), the basalt closest to the East Rift has an elevated He-3/He-4 ratio (11.3 R(sub A)), consistent with a significant plume component. The diversity in isotopic signatures also indicates that homogenization of isotopic anomalies does not occur, even in this region of `super-fast' spreading. The overall He-3/He-4-Pb-206/Pb-204 and He-3/He-4-Sr-87/Sr-86 trends have positive correlations, although the high between the He and Sr isotope distribution is modeled in the context of a plume source-migrating ridge sink. During channeling of the plume toward the ridge, helium if preferentially lost from the center of the channeled plume, resulting in lower He/Pb and He/Sr concentration ratios in the high He-3/He-4 component. Mixing trajectories in He-Sr isotopic space between a LILE depleted asthenosphere and a variably degassed plume component provide a reasonably good fit to the data and may explain the isotope systematics of plume-ridge interactions in the context of modern theories of plume dynamics.

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